Origin of low oxygen isotopic compositions in alkalic lavas from Erebus volcano, Antarctica
Author:
Funder
National Science Foundation
Publisher
Elsevier BV
Subject
Geochemistry and Petrology
Reference64 articles.
1. Oxygen isotopes in mantle and crustal magmas as revealed by single crystal analysis;Bindeman;Rev. Mineral. Geochem.,2008
2. The low δ18O late-stage ferrodiorite magmas in the Skaergaard Intrusion: Result of liquid immiscibility, thermal metamorphism, or meteoric water incorporation into magma?;Bindeman;J. Geol.,2008
3. Low δ18O rhyolites from Yellowstone: magmatic evolution based on analyses of zircons and individual phenocrysts;Bindeman;J. Petrol.,2001
4. Crustal and lithospheric structure of the West Antarctic Rift System from geophysical investigations – a review;Behrendt;Glob. Planet. Change,1999
5. Ground-based thermal imaging of the lava lakes at Erebus volcano, Antarctica;Calkins;J. Volcanol. Geotherm. Res.,2008
Cited by 2 articles. 订阅此论文施引文献 订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献
1. Comments on: “Volcanism in Antarctica: An assessment of the present state of research and future directions” by Geyer et al.: J. Volc. Geother. Res. v. 444, no. 107941;Journal of Volcanology and Geothermal Research;2024-10
2. Trans-crustal structural control of CO2-rich extensional magmatic systems revealed at Mount Erebus Antarctica;Nature Communications;2022-05-30
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